Cox, B.M. & Sumbler, M.G. 2002. British Middle Jurassic Stratigraphy. Geological Conservation Review Series, No. 26, JNCC, Peterborough, ISBN 1 86107 479 4.
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B.M. Cox
The Halfway House Cutting and Quarry GCR site comprises a cutting on the northern side of the A30 road, about midway between Sherborne and Yeovil, and two adjacent old quarries — those known in the literature as 'Rock Cottage Quarry' and 'Chapel Quarry'. The site comprises localities 2, 3 and 4 of Torrens (1969a, fig. 1). Exposure in the quarries, first noted by Wright (1856), is generally now rather poor and recent accounts of the succession have concentrated on the road cutting that was excavated during the latter part of the summer of 1963 (Torrens, 1969a; Whicher, 1969). The locality is particu larly famous for the so-called 'Halfway House Fossil Bed' (Buckman, 1893a), the ammonite assemblage of which is taken as typical of the Truellei Subzone (Upper Bajocian Parkinsoni Zone).
The Halfway House Cutting and Quarry GCR site has been well established in the literature since J. Buckman (1877), although it does not feature prominently in the recent published reviews of the Inferior Oolite Formation in this area (e.g. Callomon and Chandler, 1990). Sections at both the Rock Cottage and Chapel quarries were reported by Buckman (1893a) (his sections IV and V respectively) and Richardson (1932) (his sections 17 and 17a respectively). A composite section, based on Richardson (1932), through the whole of the Inferior Oolite Formation and the Bajocian Stage here was reported by Macfadyen (1970). Other records include those of Woodward (1894), Wilson et al. (1958) and Callomon and Cope (1995). Part of the section at Chapel Quarry was illustrated by Richardson et al. (1911, pl. )00CCX, fig. 1).
The section given below is based on that recorded by Torrens (1969b), Whicher (1969) and Callomon and Cope (1995) in the road cutting on the A30.
| Thickness (m) | |
| Inferior Oolite Formation | |
| Crackment Limestone Member | |
| 10: Limestone, white, chalky with marl partings | seen |
| 9: Limestone, grey-brown, sandy, marly; poorly fossiliferous and much stained with limonite; becoming more massive towards base; ammonites (Parkinsonia); brachiopods (Acanthothiris); echinoids (Collyrites, Pygomalus and Pygorhytis) | seen to 4.0 |
| 8: Halfway House Fossil Bed: Limestone, ooidal, very fossiliferous with ammonites (including Cadomites, Leptosphinctes, Parkinsonia and Strigoceras); nautiloids; echinoids; bivalves | 0.25 |
| 7: Astarte Bed: Limestone, ooidal, brown, limonite-stained with lirponitic concretions; many fossils coated in limonite and encrusted with serpulids; Neocrassina very common together with other bivalves, gastropods and ammonites | 0.10–0.30 |
| Irony Bed | |
| 6: Limestone, crystalline, iron-stained, ooidal in places, lensoid; thick layer of limonite at top; conglomeratic at base; ammonites (Caumontisphinctes); gastropods; abundant brachiopods | 0–0.25 |
| 5: Limestone, pale-brown to blue-hearted, ooidal; ammonites, including Graphoceras; belemnites; bivalves; Homoeorhynchia ringens (von Buch) in basal 0.10 m | 1.20–1.30 |
| Dew Bed | |
| 4: Limestone, very hard, grey, crystalline with shell debris; top surface encrusted by oysters and extensively bored by Lithophaga and thin, vertical annelid borings | 0.30 |
| 3: Fissure-filling from Bed 5 above; ooidal matrix with some limonite concretions and pebbles | 0–0.15 |
| 2: As Bed 4 above | 0.50 |
| Lias Group | |
| Bridport Sand Formation | |
| 1: Sand, soft, friable, micaceous | seen to 2.0 |
Wright (1860) first used the name Dew Bed (beds 2–4 above) for the hard, crystalline limestone at the base of the Inferior Oolite Formation hereabouts. It is also present in the Bradford Abbas Railway Cutting (see GCR site report, this volume) where it is assigned to the Lower Jurassic Toarcian Stage. Torrens (1969b) tentatively assigned the Dew Bed at the Halfway House Cutting and Quarry GCR site to the Levesquei Zone, Moorei Subzone of the latter stage and it therefore seems appropriate to assign the sands of the underlying Bed 1 there to the Bridport Sand Formation of the Lias Group; Wilson et al. (1958) and Macfadyen (1970) included the Dew Bed itself in that group.
According to Richardson et al. (1911), the quarrymen called Bed 5 'the Blue Beds'. The presence of the brachiopod Homoeorhynchia ringens in its basal part is indicative of the Ringens Bed (see Holway Hill Quarry and Louse Hill Quarry GCR site reports, this volume). Davidson (1878) described the species as being abundant and two of his three figured specimens came from here (see
The Irony Bed (Bed 6) is well developed in this area (see Seavington St Mary Quarry, Bradford Abbas Railway Cutting and Louse Hill Quarry GCR site reports, this volume). It appears to be locally diachronous within the Lower Bajoican Sauzei and Humphriesianum zones (Parsons, 1980a; see Louse Hill Quarry GCR site report, this volume), although the record of Caumontisphinctes at the Halfway House Cutting and Quarry GCR site, if correct, would also imply the Upper Bajocian Subfurcatum Zone. There is a substantial non-sequence at the base of the bed where at least the Discites, Ovalis and Laeviuscula zones are missing.
The Astarte Bed (Bed 7) is generally recognized as the oldest Upper Bajocian stratum present in this area, where it is known at several localities (e.g. Louse Hill Quarry, see GCR site report, this volume). Its ammonites indicate the Garantiana Zone although, within that zone, it appears to be diachronous. Ammonites at Louse Hill Quarry indicate the Dichotoma Subzone (Callomon and Cope, 1995) but at Seavington St Mary Quarry, it has been assigned to the Acris Subzone (Parsons, 1980a). The bivalve that gives its name to the bed is now referred to the genus Neocrassina (see Burton Cliff and Cliff Hill Road Section GCR site report, this volume).
The highest beds (8–10) of the section, with the ammonite Parkinsonia, are assigned to the Upper Bajocian Parkinsoni Zone. Bed 8 (the Halfway House Fossil Bed — a term first used by Buckman, 1893a) is the type horizon for the Truellei Subzone (Buckman, 1891; Arkell, 1951a). The fauna of this very fossiliferous bed is the same as that of the Truellei Bed at Burton Bradstock (see Burton Cliff and Cliff Hill Road Section GCR site report, this volume). It includes large specimens of the ammonites Leptosphinctes meseres (S.S. Buckman) and Parkinsonia dorsetensis (Wright)
The Halfway House Cutting and Quarry GCR site displays nearly the whole of the local Aalenian–Bajocian succession, albeit very attenuated, with its characteristic 'hardgrounds', conglomerates and thin, lenticular 'iron-shot' limestones. It includes a number of significant non-sequences and the zonal succession is even less complete than at the nearby Bradford Abbas Railway Cutting and Louse Hill Quarry GCR sites with which it otherwise has features in common. The Halfway House Fossil Bed is particularly famous and provides the type horizon for the Truellei Subzone of the Upper Bajocian Parkinsoni Zone. Sited in an area of complex Aalenian–Bajocian stratigraphy, the Halfway House Cutting and Quarry locality is thus an important one for the interpretation of the local and regional succession as well as for correlations farther afield.